毫米波宽带低副瓣波导缝隙阵列天线设计

本文提出了一种毫米波宽带低副瓣波导缝隙阵列天线。该天线分为上下两层,利用下层的功分器和反相器使电磁波从上层的辐射波导的两端向中心进行馈电,激励12个非均匀波导缝隙辐射单元。该天线呈中心对称结构,结构紧凑,并使得天线的方向图具有稳定性。在辐射波导中引入二阶短路金属阶梯,并且阵列的辐射单元采用非连续的双层缝隙,拓展了天线的工作带宽。所提出的加载二阶金属阶梯双层缝隙阵列天线的阻抗带宽达到16.3%(35.35~41.55 GHz),峰值增益为16 dBi,工作频带内天线的增益下降低于2.5 dBi,副瓣电平低于-20 dB。     

GRACE gravity field modeling with an investigation on correlation between nuisance parameters and gravity field coefficients

The GRACE (Gravity Recovery And Climate Experiment) monthly gravity models have been independently produced and published by several research institutions, such as Center for Space Research (CSR), GeoForschungsZentrum (GFZ), Jet Propulsion Laboratory (JPL), Centre National d’Etudes Spatiales (CNES) and Delft Institute of Earth Observation and Space Systems (DEOS). According to their processing standards, above institutions use the traditional variational approach except that the DEOS exploits the acceleration approach. The background force models employed are rather similar. The produced gravity field models generally agree with one another in the spatial pattern. However, there are some discrepancies in the gravity signal amplitude between solutions produced by different institutions. In particular, 10%–30% signal amplitude differences in some river basins can be observed. In this paper, we implemented a variant of the traditional variational approach and computed two sets of monthly gravity field solutions using the data from January 2005 to December 2006. The input data are K-band range-rates (KBRR) and kinematic orbits of GRACE satellites. The main difference in the production of our two types of models is how to deal with nuisance parameters. This type of parameters is necessary to absorb low-frequency errors in the data, which are mainly the aliasing and instrument errors. One way is to remove the nuisance parameters before estimating the geopotential coefficients, called NPARB approach in the paper. The other way is to estimate the nuisance parameters and geopotential coefficients simultaneously, called NPESS approach. These two types of solutions mainly differ in geopotential coefficients from degree 2 to 5. This can be explained by the fact that the nuisance parameters and the gravity field coefficients are highly correlated, particularly at low degrees. We compare these solutions with the official and published ones by means of spectral analysis. It is found that our solutions are, in general, consistent with others in the spatial pattern. The water storage variations of the Amazon, Chari and Ganges river basins have also been computed. The variations computed with the NPARB approach are closer to those produced by JPL and DEOS solutions, while the variations produced with the NPESS approach are in good agreement with those produced by the CSR and GFZ solutions. A simulation study is implemented with considering realistic noise and low-frequency error. The two approaches are used to recover the true model. The NPESS solution appears closer to the true one. Therefore we are inclined to estimate the nuisance parameters simultaneously with the geopential coefficients.     

A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles

The Global Positioning System (GPS) Radio Occultation (RO) technique has global coverage and is capable of generating high vertical resolution temperature profiles of the upper troposphere and lower stratosphere with sub-Kelvin accuracy and long-term stability, regardless of weather conditions. In this work, we take advantage of the anomalously high density of occultation events at the eastern side of the highest Andes Mountains during the initial mission months of COSMIC (Constellation Observing System for Meteorology, Ionosphere and Climate). This region is well-known for its high wave activity. We choose to study two pairs of GPS RO, both containing two occultations that occurred close in time and space. One pair shows significant differences between both temperature profiles. Numerical simulations with a mesoscale model were performed, in order to understand this discrepancy. It is attributed to the presence of a horizontal inhomogeneous structure caused by gravity waves.     

Gravity wave momentum flux generation close to mid-latitude Andes in mesoscale simulations of late 20th and 21st centuries

Adequate representations of diverse dynamical processes in general circulation models (GCM) are necessary to obtain reliable simulations of the present and the future. The parameterization of orographic gravity wave drag (GWD) is one of the critical components of GCM. It is therefore convenient to evaluate whether standard orographic GWD parameterizations are appropriate. One alternative is to study the generation of gravity waves (GW) with horizontal resolutions that are higher than those used in current GCM simulations. Here we assess the seasonal pattern of topographic GW momentum flux (GWMF) generation for the late 20th and 21st centuries in a downscaling using the Rossby Centre regional atmospheric model under the Intergovernmental Panel on Climate Change A1B emission conditions. We focus on one of the world’s strongest extra-tropical GW zones, the Andes Mountains at mid-latitudes in the Southern Hemisphere. The presence of two GCM sub-grid scale structures locally contributing to GWMF (one positive and one negative) is found to the East of the mountains. For the late 21st century the strength of these structures during the GW high season increases around 23% with respect to the late 20th century, but the GWMF average over GCM grid cell scales remains negative and nearly constant around −0.015 Pa. This constitutes a steady significant contribution during GW high season, which is not related to the GWMF released by individual sporadic strong GW events. This characteristic agrees with the fact that no statistically significant variation in GWMF at source level has been observed in recent GCM simulations of atmospheric change induced by increases in greenhouse gases.     

基于模态反转的半球谐振陀螺零位自校准方法

针对半球谐振陀螺的零位漂移问题,本文研究了基于模态反转电路控制技术的零位自校准方法。首先,从动力学模型引入阻尼不对称、频率裂解等非理想因素,讨论半球谐振陀螺的工作机理及驻波漂移特性。其次,通过理论分析模态反转的零位校准以及虚拟进动控制的模态反转技术。最后,基于FPGA数字控制平台,设计并实现了半球谐振陀螺零位自校准半实物仿真实验。实验结果表明,基于模态反转的半球谐振陀螺零位校准,实现了半球谐振陀螺的零位从15 降低至2 ,短期零偏稳定性和长期稳定性也分别提高了11.8％和45.86％,有效地抑制了零位漂移,提高了半球谐振陀螺测量精度。     

确定无约束梁耦合振型的一种途径

无约束梁耦合振动问题属于单柔体动力学问题,确定无约束梁耦合振型对于分析梁的振动性质具有重要意义。首先给出单柔体动力学的拟变分原理,然后分析无约束梁耦合振动的特点,应用单柔体动力学的拟变分原理建立了确定无约束梁耦合振型的一种途径。应用这种途径求解无约束梁耦合振动的奇数次振型和偶数次振型。最后,讨论了有关问题。     

Coupled Stress-Electricity Model for Electromagnetic Emission Induced by Concrete Fracture

Electromagnetic emission induced during concrete fracturing is of great significance to health monitoring of concrete structures.A coupled stress-electricity model is established by analyzing the interaction between stress and electricity during concrete fracturing.And based on this model,the electromagnetic radiation parameters are calculated.The theoretical calculation is well coincident with experimental results.This work provides theoretical support for concrete testing system.     

液固撞击的非线性耦合波动模型研究

推导了可用于研究液固撞击问题的非线性耦合波动模型 ,并将其应用于球形液滴与弹性固体平面撞击过程的数值分析。细致地研究了液固接触面及液体内无量纲压力分布 ,固体区域内等效应力的分布 ,固体弹性对撞击过程的影响 ,以及各个计算时层固体区域内最大等效应力所在点的位置。分析结果表明非线性波动模型可以较为准确地描述液固撞击过程 ,给出详细的液固撞击过程的各个物理参量 ;为液滴侵蚀固体表面问题的研究提供了可靠的基础。     

高超音速湍流分离激波结构不稳定性的实验研究

用铂膜电阻温度计测量了前向台阶诱导激波与湍流边界层相互作用流场中的表面热流率脉动。试验条件是:自由流马赫数为7.8,单位长度雷诺数为3.5×10~7米~(-1)。给出相互作用区平均热流率和脉动热流率分布。结果表明:在激波诱导的高超音速湍流分离流中,激波结构是不稳定的,产生一个间歇区域。在间歇区中,表面平均热流率由未扰动湍流边界层的热流信号和低频高幅热流脉动迭加而成,出现一个极大值。相互作用愈强,愈大,间歇区域愈长。     

蛇形进气道的雷达截面分析

 本文采用复射线技术的原理和方法,通过场的高斯波束拟合,使这种理论能够用于进气道之类的大口径凹形腔体的雷达截面(RCS)特性分析。本文以弯曲的蛇形进气道为例,进行了RCS特性分析计算,并将计算值与测试值比较。结果表明,这种方法是一种比较准确而又十分有效的RCS预估方法。